Lithologic Reservoirs ›› 2013, Vol. 25 ›› Issue (5): 49-58.doi: 10.3969/j.issn.1673-8926.2013.05.009

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Sequence stratigraphic framework and source-reservoir-caprock assemblage of Yanchang Formation in western Nanliang area, Ordos Basin

ZHAO Tianlin 1,2, LUO Jinglan2, DENG Yuan1, LI Miao2, BAI Xuejing2, GUO Tao3   

  1. 1. Shaanxi Nuclear Industry Geology Surveying Institute, Xi’an 710054, China; 2. State Key Laboratory of Continental Dynamics,Northwest University, Xi’an 710069, China; 3. 185 Team, Shaanxi Coalfield Geology Bureau, Yulin 719000, China
  • Online:2013-09-26 Published:2013-09-26

Abstract:

In order to study sequence stratigraphic framework and source-reservoir-caprock assemblage of Upper Triassic Yanchang Formation in western Nanliang area, this paper studied the sequence boundary types, the characteristics of sequence stratigraphic framework, and the relationship between long-term base-level cycle and source-reservoir caprock assemblage by the theory and approach of high resolution sequence stratigraphy. The result shows that five third-order sequence boundaries are identified, the Yanchang Formation consist of four long-term and one super-long term base-level cycles. The source-reservoir-caprock assemblage has close relation to the long-term base-level cycle. The sand bodies of delta plain distributary channel and front underwater distributary channel developed in the early middle stage of the uprising periods and middle-late stage of subsiding periods are high quality reservoir, the turbidite sand bodies developed in the middle-late stage of the uprising periods and early-middle stage of subsiding periods are potential reservoir, and the lacustrine shale and carbon mudstone developed in the surrounding of transforming interface of uprising to subsiding of the long-term base-level cycle. The Yanchang Formation developed three types of source-reservoir-caprock assemblage, including upper-sourcing and lower-reservoir type and lower-sourcing and upper reservoir type and self-sourcing and self-reservoir type.

Key words: extra-highwater cut stage, liquid-oil ratio, water drive curve, forecastingmodel

[1] Cross T A,Lessenger M A. Sediment volume partitioning:Rationale for stratigraphic model evaluation and high-resolution stratigraphic correlation[R]. Accepted for publication in Norwegian Petroleums-Forening Conference Volume,1996:1-24.
[2] Currie B S. Sequence stratigraphy of nonmarine Jurassuc-Cretaceous rocks,central Cordillenan foreland-basin system[J]. Geological Society of America Bulletin,1997,109(9):1206-1222.
[3] Martinsen O J,Ryseth A,Helland Hansen W,et al. Stratigraphic base level and fluvial architecture Ericson sandstone(Campanian),rock springs uplift,SW Wyoming USA[J]. Sedimentology,1999,46(2):235-259.
[4] 罗静兰,Marcelo J K,李文厚,等.延长油区侏罗系上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4):337-341.
[5] 兰朝利,吴峻,李继亮,等.靖安油田长6 段层序地层分析[J].石油与天然气地质,2001,22(4):362-366.
[6] 郑荣才,彭军.陕北志丹三角洲长6 油层组高分辨率层序分析与等时对比[J].沉积学报,2002,20(1):92-100.
[7] 王宏波,郑希民,冯明.鄂尔多斯盆地三叠系延长组层序地层与生储盖组合特征[J].天然气地球科学,2006,17(5):677-681.
[8] 郭艳琴,李文厚,陈全红,等.陇东地区延长组层序地层特征及油气勘探意义[J].中国地质,2007,34(3):406-411.
[9] 王峰,田景春,陈蓉.盐定地区三叠系延长组层序地层特征与生储盖组合[J].新疆地质,2007,25(1):96-100.
[10] 倪新峰,陈洪德,韦东晓.鄂尔多斯盆地三叠系延长组层序地层格架与油气勘探[J].中国地质,2007,34(1):73-79.
[11] 徐丽,王轶平,段毅,等.鄂尔多斯盆地南梁地区长4+5 油层组储层特征[J].岩性油气藏,2012,24(4):34-39.
[12] 刘犟,李凤杰,侯景涛,等.鄂尔多斯盆地吴起地区下侏罗富县组沉积相特征[J].岩性油气藏,2012,24(3):74-78.
[13] 王力,崔攀峰.鄂尔多斯盆地西峰油田长8 沉积相研究[J].西安石油学院学报:自然科学版,2003,18(6):26-30.
[14] 黄龙,田景春,王峰.富县地区延长组高分辨率层序地层分析[J].岩性油气藏,2012,24(6):88-93.
[15] 苏德辰,李庆谋,罗光文,等.Fischer 图解及其在旋回层序研究中的应用———以北京西山张夏组为例[J].现代地质,1995,9(3):279-283.
[16] 翟永红.用Fischer 图解研究山西临汾中奥陶世马家沟组旋回层序[J].岩石矿物学杂志,1999,28(2):128-133.
[17] 王起琮,李文厚,赵靖舟,等.陕北地区三叠系延长组长1 段烃源岩生物标志化合物特征[J].中国西部油气地质,2006,2(2):194-198.
[18] 邓宏文,王洪亮,祝永军,等.高分辨率层序地层学———原理及应用[M].北京:地质出版社,2002:49-50.
[19] 李君文.基准面旋回与储层宏观非均质性的关系[J].岩性油气藏,2011,23(3):29-39.
[20] 朱宗良,李克永,李文厚,等.鄂尔多斯盆地上三叠统延长组富油因素分析[J].地质科技情报,2010,29(3):75-78.
[21] 梁晓伟,王海红,牛小兵,等.鄂尔多斯盆地中西部延长组烃源岩评价及油源对比[J].成都理工大学学报:自然科学版,2011,38(4):402-407.
[22] 师磊,卢双舫,李吉军,等.鄂尔多斯盆地长9 烃源岩评价[J].科学技术与工程,2011,11(20):4756-4761.
[23] 屈红军,杨县超,曹金舟,等.鄂尔多斯盆地上三叠统延长组深层油气聚集规律[J].石油学报,2011,32(2):243-248.
[24] 郭艳琴,李文厚,陈全红,等.鄂尔多斯盆地安塞—富县地区延长组—延安组原油地球化学特征及油源对比[J].石油与天然气地质,2006,27(2):218-224.
[25] 张晓丽,段毅,何金先,等.鄂尔多斯盆地华庆地区延长组下油层组原油地球化学特征及油源对比[J].天然气地球科学,2011,22(5):866-873.
[26] 白玉斌,罗静兰,张天杰,等.鄂尔多斯盆地吴堡地区延长组烃源岩特征及评价[J].兰州大学学报:自然科学版,2012,48(5):22-23.
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